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Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint

GlacierEngineeringPaleoenvironmental ChangePast 104GeographyGreenland GripGeologyCryosphereGeochemistryGlacial ProcessGeochronologyPaleoclimatologyEarth ScienceNgrip Ice Cores